Two-dimensional Numerical Simulations of Mixing under Ice Keels

Changes in sea ice conditions directly impact the way the wind transfers energy to the Arctic Ocean. The thinning and increasing mobility of sea ice is expected to change the size and speed of ridges on the underside of ice floes, called ice keels, which cause turbulence and impact upper-ocean strat...

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Main Authors: Abreu, Sam, Cormier, Rosalie M., Schee, Mikhail G., Zemskova, Varvara E., Rosenblum, Erica, Grisouard, Nicolas
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-1756
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1756/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere113624 2023-10-09T21:48:46+02:00 Two-dimensional Numerical Simulations of Mixing under Ice Keels Abreu, Sam Cormier, Rosalie M. Schee, Mikhail G. Zemskova, Varvara E. Rosenblum, Erica Grisouard, Nicolas 2023-09-14 application/pdf https://doi.org/10.5194/egusphere-2023-1756 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1756/ eng eng doi:10.5194/egusphere-2023-1756 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1756/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-1756 2023-09-18T16:24:16Z Changes in sea ice conditions directly impact the way the wind transfers energy to the Arctic Ocean. The thinning and increasing mobility of sea ice is expected to change the size and speed of ridges on the underside of ice floes, called ice keels, which cause turbulence and impact upper-ocean stratification. However, the effects of changing ice keel characteristics on below-ice mixing are difficult to determine from sparse observations and have not been directly investigated in numerical or laboratory experiments. Here, for the first time, we examine how the size and speed of an ice keel affect the mixing of various upper-ocean stratifications using 16 two-dimensional numerical simulations of a keel moving through a two-layer flow. We find that the irreversible ocean mixing and the characteristic depth over which mixing occurs each vary significantly across a realistic parameter space of keel sizes, keel speeds, and ocean stratifications. Furthermore, we find that mixing does not increase monotonically with ice keel depth and speed, but instead depends on the emergence and propagation of vortices and turbulence. These results suggest that changes to ice keel speed and depth may have a significant impact on below-ice mixing across the Arctic Ocean, and highlight the need for more realistic numerical simulations and observational estimates of ice keel characteristics. Text Arctic Arctic Ocean Sea ice Copernicus Publications: E-Journals Arctic Arctic Ocean
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Changes in sea ice conditions directly impact the way the wind transfers energy to the Arctic Ocean. The thinning and increasing mobility of sea ice is expected to change the size and speed of ridges on the underside of ice floes, called ice keels, which cause turbulence and impact upper-ocean stratification. However, the effects of changing ice keel characteristics on below-ice mixing are difficult to determine from sparse observations and have not been directly investigated in numerical or laboratory experiments. Here, for the first time, we examine how the size and speed of an ice keel affect the mixing of various upper-ocean stratifications using 16 two-dimensional numerical simulations of a keel moving through a two-layer flow. We find that the irreversible ocean mixing and the characteristic depth over which mixing occurs each vary significantly across a realistic parameter space of keel sizes, keel speeds, and ocean stratifications. Furthermore, we find that mixing does not increase monotonically with ice keel depth and speed, but instead depends on the emergence and propagation of vortices and turbulence. These results suggest that changes to ice keel speed and depth may have a significant impact on below-ice mixing across the Arctic Ocean, and highlight the need for more realistic numerical simulations and observational estimates of ice keel characteristics.
format Text
author Abreu, Sam
Cormier, Rosalie M.
Schee, Mikhail G.
Zemskova, Varvara E.
Rosenblum, Erica
Grisouard, Nicolas
spellingShingle Abreu, Sam
Cormier, Rosalie M.
Schee, Mikhail G.
Zemskova, Varvara E.
Rosenblum, Erica
Grisouard, Nicolas
Two-dimensional Numerical Simulations of Mixing under Ice Keels
author_facet Abreu, Sam
Cormier, Rosalie M.
Schee, Mikhail G.
Zemskova, Varvara E.
Rosenblum, Erica
Grisouard, Nicolas
author_sort Abreu, Sam
title Two-dimensional Numerical Simulations of Mixing under Ice Keels
title_short Two-dimensional Numerical Simulations of Mixing under Ice Keels
title_full Two-dimensional Numerical Simulations of Mixing under Ice Keels
title_fullStr Two-dimensional Numerical Simulations of Mixing under Ice Keels
title_full_unstemmed Two-dimensional Numerical Simulations of Mixing under Ice Keels
title_sort two-dimensional numerical simulations of mixing under ice keels
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-1756
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1756/
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-1756
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1756/
op_doi https://doi.org/10.5194/egusphere-2023-1756
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